A climatological study of sea breeze clouds in the southeast of the Iberian Peninsula (Alicante, Spain)
Sea breezes blow under anticyclonic weather types, weak surface pressure gradients, intense solar radiation and relatively cloud-free skies. Generally, total cloud cover must be less than 4/8 in order to cause a thermal and pressure difference between land and sea air which allows the development of...
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| Vydáno v: | Atmósfera |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Nacional Autónoma de México
2009
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=56512093002 |
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